国产激情久久久久影院小草_国产91高跟丝袜_99精品视频99_三级真人片在线观看

иxƔ}(yng)ԓô

l(f)rg:2017-10-27 ݋:1025

ͬͬWвͬLc挦иxһҪfиxʮN}ķNyǧǧ҂Ĕ(sh)(j)ĽǶȁy(tng)Ӌ͕l(f)F(xin)(sh)ͬWиxСY(ji)}Ɣ}ҪôrgҪô֪ԓxһ헣Ķ(sh)@ɷN}ͱ^҂͞ҷһ˼SQиxƔ}

fƔ}ҪҪmȻƔ}F䌍иx]ôyи˜ʻԇ϶һĴ}ик߉݋Y(ji)(gu)ÿȻǰTS (Topic Sentence) + SD (Supporting details)չ_¶ǰIntroduction + Aspects + Attitudesչ_ġֻµČ˼·ܸø}Ŀ߱ضǰһŶһˮƽS¼l(f)չƔ}׌@SϵijһcȥƜyoǾ̓ɂSl(f)չķSl(f)չķҲ҂Ҫf˼SȥQƔ}

OGόƔ}xz鿼Џҽh^f^c(stronglyimplied but not explicitly stated in the text)̶}Ŀ}ĿҪ£

Paragraph 2 suggests which of the following about X?

Which of the following can be inferred from paragraph 2 about X?

According to paragraph 3, what do Y indicate about X?

According to paragraph 4, what does the author imply about X?

}гF(xin)infer, imply, indicatesuggest@Ă~҂ж@}ĿƔ}ôƔ}(yng)ԓν?

һД}҂õ}ĿĂ~еκһо@Ɣ}Ɣ}}ּҰʾҪͨ^ƒ(ni)MкƔࡣ

ڶ}ԭĶλмx}Ū}Ƀ(ni)ݣƔ෽}ɺϢМʴ_λ

Ɯy+Д(j)P(gun)M(yu)x_

ƔࣺŒϢ}}һ𰸾ǶλľӵͬxČ

Ɣࣺ·֞ɷNһNǕrgڶNǃČ

һN}F(xin)ʾrgϢ磺after 1932, since early years ofthe 19th century. TPO 20 Passage 1 Western Migration Q1:

Paragraph 1: The story of the westward movement of population in the US is, in the main, the story of the expansion of American agriculture of the development of new areas for the raising of livestock and the cultivation of wheat, corn, tobacco, and cotton. After 1815, improved transportation enabled more and more western farmers to escape aself-sufficient way of life and enter a national market economy during periods when commodity prices were high, the rate of westward migration increased spectacularly

What can be inferred from paragraph 1 about western farmers prior to 1815?

They had limited their crop production to wheat, corn,tobacco and cotton

They were able to sell their produce at high prices

They had not been successful in raising cattle

They did not operate in a national market economy

}гF(xin)˃ɂϢһwestern farmers, һprior to 1815, ɗlϢȥжλλڵһεЛ]ᵽ1815֮ǰֻ1815֮󣬴䌍ֻܺҪ1815֮ă(ni)ݿˣ@(ni)ǰnoteεӣ“ĬF(xin)Jessicaǂ”“ՈƔJessicaôô?”ܺܶ뵽“DzJessica׃g(sh)?”䌍@^Ɣ𰸾Jessica첻ǂԚw}fƵĽͨʹԽԽr(nng)[ÓԽoMˇԵЈ(jng)ǂr؛ărܶwƵҲL

ڶNČЕF(xin)ʾȵP(gun)ϵ~by contrast, unlike, while,whereas, on the contrary, in comparison to, distinct from, different from~TPO 2еThe Origins of Cetaceansĵ2}׌ƜyP(gun)early sea ottersصԭжλl(f)F(xin)P(gun)Iдһunlike, fsea otters, һL^y(not easy=difficult)҂һ£fsea ottersLʲôӱ^_гF(xin)not difficult, @}ܺȻETSһֱ@ôεƔ}@ֻǽoһ}ķ

Paragraph 4: These ideas remain controversial.Proponents point to features such as the terraced "beaches" shown inone image, which could conceivably have been left behind as a lake or oceanevaporated and the shoreline receded. But detractors maintain that the terraces could also have been created by geological activity, perhaps related to the geologic forces that depressed the Northern Hemisphere far below the level of the south, in which case they have nothing whatever to do with Martian water. Furthermore, Mars Global Surveyor data released in 2003 seem to indicate that the Martian surface contains too few carbonate rock layers-layers containing compounds of carbon and oxygen-that should have been formed in abundance in anancient ocean. Their absence supports the picture of a cold, dry Mars that never experienced the extended mild period required to form lakes and oceans. However, more recent data imply that at least some parts of the planet did infact experience long periods in the past during which liquid water existed onthe surface

10. According to paragraph 4, what do the 2003 Global Surveyor data suggest about Mars?

Ancient oceans on Mars contained only small amounts of carbon

The climate of Mars may not have been suitable for the formation of large bodies of water

Liquid water may have existed on some parts of Mars'surface for long periods of time

The ancient oceans that formed on Mars dried up duringperiods of cold, dry weather

(j)P(gun)I~҂λĶεg֣Mars Global Surveyor data releasedin 2003 seem to indicate that the Martian surface contains too few carbon aterock layers-layers containing compounds of carbon and oxygen-that should have been formed in abundance in an ancient ocean@}ԮŒϢ}ȥעⲻԭĵĺ؏(f)suggest ԭindicateͬxD(zhun)Q҂ֻҪҵwhatͺˣԭthatcF(xin)too few, should have,

БB(ti)Ɯyһַ񶨑B(ti)ȣҲffγ an ancient ocean̫҂x헣AfAncient oceans on Mars contained onlysmall amounts of carbonwcԭìų;Bx The climate of Mars may not have been suitable for the formation oflarge bodies of waterfmγɴˮַ񶨑B(ti)ȣԭ;CxLiquid water may have existed on some parts of Mars' surface forlong periods of timeP(gun)δἰų;DxThe ancient oceans that formed on Mars dried up during periods ofcold, dry weather. fancient oceans]УԭкɺcԭIJų_𰸞B

挦иxƔ}Փ߀P(gun)IǴҪo^X¼l(f)չĕrgS¼ˮƽSMԭƔijͻc(j)ԭĵă(ni)ҳ(yng)ĸ(j)ôиxƔ}_һܺõF(xin)ھͿԌ`һ

]
T]